The ecoregion covers the Solomon Islands archipelago, which is divided between the countries of Solomon Islands and Papua New Guinea. The archipelago's northern islands, Bougainville and Buka, are part of Papua New Guinea. The rest of the archipelago is within the nation of Solomon Islands. The ecoregion excludes the eastern islands of the nation of Solomon Islands, the Santa Cruz Islands, which lie in the Vanuatu rain forests ecoregion together with the neighbouring archipelago of Vanuatu.[5] The archipelago extends approximately 1450 km from northwest to southeast, between 5° and 12° South latitude.[6]
Bougainville is the largest island, about 200 km long and from 50 to 60 km wide with an area of almost 9000 km2. The island has a central mountain range, the northern part of which is known as the Emperor Range, and the southern part, separated by a lower saddle, as the Crown Prince Range. Mount Balbi in the Emperor Range, at 2,715 metres elevation, is the highest peak in the archipelago. Volcanic rocks are common, with dating back approximately 30 million years. The Panguna mine in the Crown Prince Range, currently closed, is one of the largest copper mines on earth. The Keriaka Plateau in northwest Bougainville, south of Mount Balbi, is a karst plateau formed of weathered foraminiferouslimestone dating to the lower Miocene.[6]
The rest of the archipelago extends southeast of Bougainville as a double chain. The outer or northeastern chain comprises the islands of Choiseul, Santa Isabel, and Malaita, which are each about 200 km long and 30 km wide. The islands have mountainous interiors extending above 1000 m on Choiseul, 1200 m on Santa Isabel, and 1300 m on Malaita.[6]
Most of the inner and outer chain islands are made up of volcanic rocks, including andesite and basalt. Guadalcanal has the most complex geology, with areas of andesite volcanics, intrusive plutonic rocks, Pliocene sedimentary rocks, and uplifted Pleistocene coralline limestone in the northern lowlands near Honiara. There are outcrops of ultramafic rock, rich in chromium and nickel, on five islands – at Santa Isabel's southern tip, on the nearby island of San Jorge, in the Florida Islands, in southwestern Guadalcanal, and in north-central San Cristobal. These rocks are toxic to many plants, and are often home to distinctive plant communities.[6]
The archipelago includes two groups of low coralline outlying islands – Ontong Java, northeast of the outer chain and 450 km north of Honiara, and Rennell and Bellona, south of San Cristobal and 250 km south of Honiara.[6]
The islands have a humid tropical climate. Rainfall averages between 3000 and 5000 mm annually at most sea-level stations. There is little seasonal variation in temperature, with seasonal variation in rainfall depending on the prevailing winds. The southeast trade winds are active from about March to October when the sun is north of the equator. February-March and November-December are unsettled weather periods when the islands can get drenched with convectional rains. Winds come from the northwest from December to February. The southern islands can experience tropical cyclones, which usually develop between November and April. Guadalcanal's relatively high east-west running mountains create a rain shadow effect in the island's northeastern lowlands, with lower rainfall during the southwest trade wind season than elsewhere in the archipelago.[6]
Temperatures above 700 meters elevation are generally 4 to 5°C cooler than the lowlands, with mean annual temperatures of 22 to 23°C. The highlands experience cloud cover during the southeast trade wind season, and windward slopes have higher rainfall than the lowlands.[6]
Flora
Share of forest area in total land area, top countries (2021). The Solomon Islands have the sixth highest percentage of forest cover in the world.
The natural vegetation of the Solomon archipelago consists mostly of lowland and montanetropical rain forests. The major plant communities include coastal strand, mangrove forests, freshwater swamp forests, lowland rain forests, and montane rain forests. Seasonally-dry forests and grasslands are found on the northern (leeward) slopes of Guadalcanal.[7]
Montane forests in the Solomons share many species with the lowland forests, and differ primarily having a lower canopy height – 20 to 25 meters. The Solomons' montane forests are absent many of the tree species characteristic of montane forests in the Bismarcks and New Guinea, including Nothofagus (southern beech) and Fagaceae (species of Castanopsis and Lithocarpus).[6]
Above 1500 metres elevation on Bougainville the forests transition to montane scrub of Pandanus and the palm Hydriastele macrospadix, or tree fern (Cyathea sp.) and bamboo scrub on more recent volcanic deposits, with pockets of submontane forest in sheltered areas with deeper soils.[6]
In northern Guadalcanal, where the rain shadow of the mountains creates drier conditions from June to October, there are areas of mixed-deciduous forest and grassland. The mixed-deciduous forest has an open, fragmented canopy with Pometia pinnata, Vitex cofassus, and Kleinhovia hospita common. Deciduous trees include Pterocarpus indicus, Antiaris toxicaria, and species of Ficus and Sterculia. Small and understorey trees include the poisonous Semecarpus spp., Colona scabra, and Cananga odorata. Mixed-deciduous forest extends into grasssland areas as gallery forest along streams and rivers.[6]
199 bird species are native to the Solomon archipelago, of which 69 species are endemic.[7] The ecoregion corresponds to the Solomon groupendemic bird area.[8]
The first evidence of human inhabitation of the archipelago is at Kilu Cave on Buka, dating back 29,000 years ago to the Pleistocene. The settlers likely crossed the sea from the Bismarck Archipelago. At the time sea levels were lower, and New Ireland was separated from the Solomons by 180 km. The lower sea levels also joined several of the islands, including Buka, Bougainville, Choiseul, Santa Isabel, and the Florida Islands, into a single island known as Greater Bougainville or Greater Bukida.[9]
Early settlers were likely highly mobile hunter-gatherers. Evidence from Kilu Cave show that early residents hunted bats, reptiles, rats, and birds from at least six families including several species of pigeon, a megapode, and a rail, along with marine shells and fish bones indicating inshore fishing. Residents also ate starches from taro (Colocasia esculenta) and Alocasia sp. The nut-producing trees Canarium indicum and Canarium salomonense were introduced to the Solomons from the New Guinea mainland about 10,000 years ago. Sea levels rose to close to current levels between 5500 and 6000 years before present (B.P.). Lapita settlers, the ancestors of today's Oceanic Austronesian peoples, arrived by 3400 B.P., and introduced the marsupial gray cuscus (Phalanger orientalis) to the islands.[9]
The people of the Solomons today are diverse in culture and language. Between 70 and 80 languages are spoken in the archipelago. There is a cultural distinction between “salt-water” and “bush” people, with bush people dwelling inland with lifestyles and traditions centred on the forest and gardens, and “salt water” people dwelling near the coast with a lifestyle and culture oriented to the sea. In parts of the archipelago, like the Western Solomons, the island interiors are now little inhabited.[9]
Many islanders engage in subsistence gardening. Bush fallowing is common practice, rotating gardens in a confined area of forest over relatively short period, then leaving sections fallow so that shrub-forest and soil fertility can recover. Primary forest trees which produce edible nuts and fruits, including Canarium species, Barringtonia species, Artocarpus altilis, and Pangium edule, are usually retained when shrub-forest is cleared for gardens.[6]
Conservation and threats
Most of the mountain forests are relatively intact, while areas of the lowlands have been cleared for farms and gardens and plantations of coconut (Cocos nucifera) and other food, fiber, timber-producing trees. Much of the grassland east of Honiara has been replaced by plantations of oil palm (Elaeis guineensis).[6]
Commercial logging began in the 1920s, and has removed large areas of forest across the archipelago, mostly in the lowlands. Kolombangara is one of the most intensively logged islands in the archipelago. Clear-cut logging began in the 1960s, and by 2012 less than 10% of the island's primary forest remained, restricted to inaccessible ridgetops, ravines, and within the central crater.[10]
The Vanuatu rain forests are tropical and subtropical moist broadleaf forests ecoregion which includes the islands of Vanuatu, as well as the Santa Cruz Islands group of the neighboring Solomon Islands. It is part of the Australasian realm, which includes neighboring New Caledonia and the Solomon Islands, as well as Australia, New Guinea, and New Zealand.
The East Melanesian Islands, also known as the Solomons-Vanuatu-Bismarck moist forests, is a biogeographic region in the Melanesia subregion of Oceania. Biogeographically, the East Melanesian Islands are part of the Australasian realm.
The Sri Lanka montane rain forests is an ecoregion found above 1,000 m in the central highlands of Sri Lanka. Owing to their rich biodiversity, this region is considered to be a super-hotspot within endemic hotspots of global importance. These forests are cooler than lowland forests and therefore they have ideal conditions for growth of cloud forests. These forests classifications tropical sub montane forest, tropical sub-montane and tropical upper montane. Half of Sri Lanka's endemic flowering plants and 51 percent of the endemic vertebrates are restricted to these forests. More than 34 percent of Sri Lanka's endemic trees, shrubs, and herbs can only be found in this ecoregion. Twisted, stunted trees are a common sight in these forests, together with many varieties of orchids, mosses and ferns. The trees of montane rain forests grow to a height 10–15 meters, shorter than the lowland rain forest trees. These high altitude forests are the catchment area for most of Sri Lanka's major rivers.
The Trobriand Islands rain forests are a tropical moist broadleaf forest ecoregion of southeastern Papua New Guinea.
The pale mountain pigeon is a species of bird in the pigeon family Columbidae. It is endemic to the Solomon Islands archipelago, where it inhabits old-growth and secondary montane forest. It is a medium-size pigeon with an average length of 38 cm (15 in) and a weight of 310–385 g (10.9–13.6 oz). The head and neck are whitish-grey, the belly and lower breast are buffy-pink, and the vent and undertail coverts are pale grey. The upperparts are smoky-grey with darker fringes on the mantle and wing coverts. Both sexes look similar, but there can be large variation in individual appearance.
The crested cuckoo-dove is a species of bird in the pigeon family, Columbidae. First described by English zoologist John Gould in 1856, it is endemic to the Solomon Islands archipelago, where it mainly inhabits hill forests at elevations of 500–900 m (1,600–3,000 ft). It is a large and robust pigeon, with a length of 40–42 cm (16–17 in) and a distinctive pale purplish-grey crest. Adults are mainly bluish-grey, with a pale greyish-buff throat, blackish tail, and yellow-tipped reddish bill. Both sexes look alike. Juveniles lack the crest, have darker heads, and have duller wings.
The white-winged fantail or Cockerell's fantail, is a species of bird in the family Rhipiduridae. It is found in the Solomon Islands apart from the island of Malaita in the southeast of the archipelago. The white-gorgeted fantail was formerly considered as a subspecies.
The Solomon Archipelago is a terrestrial ecoregion and marine ecoregion in the Pacific Ocean. It includes the tropical ocean waters surrounding most of the Solomon Islands archipelago, and includes Bougainville Island and Buka Island of Papua New Guinea and their surrounding waters.
The Bougainville monkey-faced bat or Bougainville flying monkey is a megabat endemic to Bougainville Island of Papua New Guinea and Choiseul Island of the Solomon Islands in Melanesia. It inhabits mature forests in upland areas, within the Autonomous Region of Bougainville and Bougouriba Province.
The following outline is provided as an overview of and topical guide to Solomon Islands:
The Solomon Islands (archipelago) is an island group in the western South Pacific Ocean, north-east of Australia. The archipelago is in the Melanesian subregion and bioregion of Oceania and forms the eastern boundary of the Solomon Sea. The many islands of the archipelago are distributed across Papua New Guinea and Solomon Islands (country). The largest island in the archipelago is Bougainville Island, which is a part of the Autonomous Region of Bougainville along with Buka Island, the Nukumanu Islands, and a number of smaller nearby islands. Much of the remainder falls within the territory of Solomon Islands and include the atolls of Ontong Java, Sikaiana, the raised coral atolls of Bellona and Rennell, and the volcanic islands of Choiseul, Guadalcanal, Makira, Malaita, New Georgia, the Nggelas, Santa Isabel, and the Shortlands. The Santa Cruz Islands are not a part of the archipelago.
The Biak–Numfoor rain forests is a tropical moist forest ecoregion in Indonesia. The ecoregion covers the islands of Biak, Supiori, Numfoor, and several smaller islands, which lie in Cenderawasih Bay north of Yapen and New Guinea.
The Samoan tropical moist forests are a tropical moist broadleaf forest ecoregion in the Samoan Islands of the Pacific Ocean.
Kilu Cave is a paleoanthropological site located on Buka Island in the Autonomous Region of Bougainville, Papua New Guinea. Kilu Cave is located at the base of a limestone cliff, 65 m (213 ft) from the modern coastline. With evidence for human occupation dating back to 30,000 years, Kilu Cave is the earliest known site for human occupation in the Solomon Islands archipelago. The site is the oldest proof of paleolithic people navigating the open ocean i.e. navigating without land in sight. To travel from Nissan island to Buka requires crossing of at least 60 kilometers of open sea. The presence of paleolithic people at Buka therefore is at the same time evidence for the oldest and the longest paleolithic sea travel known so far.
The Sulawesi montane rain forests is a tropical moist forest ecoregion in Indonesia. It includes the highlands of Sulawesi.
The Vogelkop–Aru lowland rain forests is a tropical moist forest ecoregion in Indonesia. The ecoregion covers the peninsular lowlands of western New Guinea, along with the Aru Islands and other nearby islands.
The New Britain–New Ireland montane rain forests is a tropical moist forest ecoregion in Papua New Guinea. The ecoregion includes the mountain rain forests on the islands of New Britain and New Ireland, which lie northeast of New Guinea.
The Tongan tropical moist forests is a tropical and subtropical moist broadleaf forests ecoregion that includes the Tonga archipelago and Niue.
The Society Islands tropical moist forests is a tropical and subtropical moist broadleaf forests ecoregion in the Society Islands of French Polynesia.
The Carolines tropical moist forests is a tropical and subtropical moist broadleaf forests ecoregion in Micronesia. It includes the central and eastern Caroline Islands in the Federated States of Micronesia.
References
↑ Eric Dinerstein, David Olson, et al. (2017). An Ecoregion-Based Approach to Protecting Half the Terrestrial Realm, BioScience, Volume 67, Issue 6, June 2017, Pages 534–545; Supplemental material 2 table S1b.
1 2 Wikramanayake, Eric; Eric Dinerstein; Colby J. Loucks; et al. (2002). Terrestrial Ecoregions of the Indo-Pacific: a Conservation Assessment. Washington, DC: Island Press
↑ BirdLife International (2020) Endemic Bird Areas factsheet: Solomon group. Downloaded from http://www.birdlife.org on 02/06/2020.
1 2 3 Walter, Richard & Sheppard, Peter. (2009). A review of Solomon Island archaeology.
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